Structural Controls on Fault Slip Models of the 6 February 2023 Kahramanmaraş, Türkiye Earthquake Doublet With Finite Element Analyses

被引:0
|
作者
Tung, Sui [1 ]
Sippl, Christian [2 ]
Shirzaei, Manoochehr [3 ]
Taymaz, Tuncay [4 ]
Masterlark, Timothy [5 ]
Medved, Irina [6 ]
机构
[1] Texas Tech Univ, Lubbock, TX 79409 USA
[2] Czech Acad Sci, Prague, Czech Republic
[3] Virginia Tech, Blacksburg, VA USA
[4] Istanbul Tech Univ, Istanbul, Turkiye
[5] South Dakota Sch Mines & Technol, Rapid City, SD USA
[6] Novosibirsk State Univ, Novosibirsk, Russia
基金
欧洲研究理事会;
关键词
Kahramanmaras earthquake; structural controls; inversion; geodesy; finite element; T & uuml; rkiye; SEISMIC VELOCITY STRUCTURE; YUSHU EARTHQUAKE; STRESS CHANGES; DEFORMATION; CALIFORNIA; AMATRICE; QINGHAI; GORKHA; CHINA;
D O I
10.1029/2023GL107472
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Two major earthquakes of Mw7.8 and Mw7.5 ruptured the Southern East Anatolian Fault (SEAF) and the Savrun-& Ccedil;ardak-S & uuml;rg & uuml; fault (SCSF), devastating southeast T & uuml;rkiye and northwest Syria on 6 February 2023. We adopt innovative nonlinear and linear approaches to analyze the coseismic ground displacements and estimate the complex slip geometry. Unlike conventional analytical solutions that simplify crust heterogeneity, finite-element fault models invert the displacement data and simulate the dual-fault geometry with non-uniformly distributed shallow crustal materials. Our results suggest the west-dipping SEAF and north-dipping SCSF accommodate earthquake slips of >10 m. Their respective slip distributions and proximal aftershocks correlate spatially with local seismic velocity anomalies (i.e., Delta Vp and Delta Vs), which implies differences in structural control along these two faults and provides insights into assessing the seismic hazard of mixed incipient-mature fault systems.
引用
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页数:11
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